Abstract
Ross Sea is a broad embayment, approximately 1500 km wide and 900 km long, on the Antarctic coast (Fig. 1). Depths range from less than 300 m to greater than 1200 m and average in excess of 500 m. Bathymetry is dominated by a series of roughly northeast-southwest ridges and troughs. The continental shelf is foredeepened; the inner shelf is deeper than the outer shelf due to a combination of enhanced glacial scour and isostatic loading. Repeated expansion of the East and West Antarctic ice sheets is interpreted to have modified the continental shelf. The records of the most recent glacial expansions are preserved in the surficial features and sedimentary deposits of the Ross Sea floor.
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References
Anderson, J.B., S.S. Shipp, L.R. Bartek, and D.E. Reid, Evidence for a grounded ice sheet on the Ross Sea continental shelf during the late Pleistocene and preliminary paleodrainage reconstruction, in Contributions to Antarctic Research III, Antarctic Research Series, Volume 57, edited by D.H. Elliot, pp. 39–62, American Geophysical Union, Washington, D.C., 1992.
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Domack, E.W., M. Hilfinger, J. Franceschini, K. Licht, A. Jennings, J. Andrews, S. Shipp, and J.B. Anderson, New stratigraphic evidence from the Ross Sea continental shelf for instability of the West Antarctic Ice Sheet during the last glacial maximum (abstract), Society of Economic Paleontologists and Paleontologists, First Congress on Sedimentary Geology, Congress Program and Abstracts, 1, 46–47, 1995.
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© 1997 Chapman & Hall
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Shipp, S., Anderson, J.B. (1997). Lineations on the Ross Sea Continental Shelf, Antarctica. In: Davies, T.A., et al. Glaciated Continental Margins. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5820-6_16
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DOI: https://doi.org/10.1007/978-94-011-5820-6_16
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-412-79340-0
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